Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration

YAN Jiayong; LÜ Qintian; LUO Fan; CHEN Anguo; YE Gaofeng; ZHANG Yongqian; ZHANG Kun; ZHAO Jinhua; ZHANG Chong; LIU Zhendong; LIU Yan

doi:10.12029/gc20190402

GEOLOGY IN CHINA > 2019 > 46(4): 690-703. > DOI: 10.12029/gc20190402

YAN Jiayong, LÜ Qintian, LUO Fan, CHEN Anguo, YE Gaofeng, ZHANG Yongqian, ZHANG Kun, ZHAO Jinhua, ZHANG Chong, LIU Zhendong, LIU Yan. Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration[J]. GEOLOGY IN CHINA, 2019, 46(4): 690-703. DOI: 10.12029/gc20190402

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Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration

YAN Jiayong^{1, 2,},
LÜ Qintian^{1, 2, 3, ,},
LUO Fan^{3, 1},
CHEN Anguo⁴,
YE Gaofeng⁵,
ZHANG Yongqian^{1, 2},
ZHANG Kun^{1, 2},
ZHAO Jinhua^{1, 2},
ZHANG Chong^{1, 2},
LIU Zhendong^{1, 2},
LIU Yan^{1, 2}

1.
Chinese Academy of Geological Sciences, Beijing, 100037, China
2.
China Deep Exploration Center, China Geological Survey & Chinese Academy of Geological Sciences, Beijing, 100037, China
3.
School of Geophysics and Measurement-control Technology, East China Institute of Technology, Nanchang 330013, Jiangxi, China
4.
Geological Survey of Anhui Province, Hefei 230001, Anhui, China
5.
School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China

Funds:

China Geological Survey Program DD20160082

China Geological Survey Program DD20190012

National Key R&D Program of China 2016YFC0600201

National Natural Science Foundation 41574133

National Natural Science Foundation 41630320

More Information

Author Bio:
YAN Jiayong, male, born in 1977, doctor, senior engineer, majors in mineral detecting and deep earth exploration; E-mail: yanjy@163.com
Corresponding author:
LÜ Qingtian, male, born in 1964, doctor, professor, majors in deep earth exploration; E-mail:lqt@cags.ac.cn
Received Date: March 04, 2019
Revised Date: July 29, 2019
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

The suture zone between the Yangtze Paleoplate and the Cathaysia Paleoplate (called Qin-Hang junction belt) is one of the most important tectonic-magmatic-metallogenic belts in southeastern China. There is still considerable controversy over the method of dividing the location and boundary of the western section of the Qin-Hang junction belt. In order to identify and determine the boundaries of the Qin-Hang junction belt, the authors employed the large-scale satellite gravity and magnetic data in combination with the integrated processing and analysis of regional magnetotelluric and broadband seismic data. The comprehensive evaluation shows that the Qin-Hang junction belt is the southern boundary of the Jiangnan orogenic belt. The authors hold that the border is Ningbo-Jinhua-Shangrao-Ganzhou-Chenzhou-Beihai in the south and Shanghai-Huzhou-Yingtan-LinchuanPingxiang-Hengyang-Yongzhou-Guilin-Wuzhou-Qinzhou in the north. On both sides of the joint belt, both the gravity field and the magnetic field have distinct characteristics, indicating the different material compositions and basements between the Yangtze and Cathaysia plates. There are also local differences in the geophysical fields of the Qin-Hang junction belt, suggesting that the tectonic belt has undergone multiple stage magmatism and formed different combinations of metal deposits in different sections, forming a unique metallogenic belt, i.e., the Qin-Hang metallogenic belt.

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References (69)

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Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration